不同复垦模式下铁尾矿坡面产流产沙与水力特性

    Effects of different reclamation patterns on surface runoff, sediment yield and hydraulic characteristics of slopes in iron ore tailings

    • 摘要: 为了揭示降雨条件下铁尾矿复垦坡面的产流产沙特征与水力特性,该文采用室内人工模拟降雨方法研究了不同降雨强度(60、90、120 mm/h)和不同复垦模式(T,铁尾矿;TSH,铁尾矿与高比例生土;TM,铁尾矿与菌糠;TSM,铁尾矿、菌糠与生土;TSL,铁尾矿与低比例生土;植被类型均为胡枝子)25°坡度条件下的侵蚀过程。结果表明:1)产流速率在降雨初期迅速增长,中后期趋于稳定。添加菌糠的复垦模式产流速率高于未添加菌糠的复垦模式;2)产沙速率随降雨历时变化呈现两种模式,添加菌糠的复垦模式为减少型,未添加菌糠的复垦模式为增加型,TSL的减沙效果最为显著,T对降雨强度的响应最为敏感且高雨强下产沙量最大;3)所有复垦坡面平均径流深度范围在0.23~0.93 mm,水流流态均为层流,大部分情况下水流流型为缓流,但TSH在中高雨强下以及T在高雨强下为急流。添加菌糠模式的曼宁糙率系数和水流阻力系数高于未添加菌糠的复垦模式,流速低于未添加菌糠的复垦模式,添加菌糠的基质表面粗糙度较大;4)各复垦坡面的侵蚀形式以溅蚀和片蚀为主,高雨强下T出现细沟侵蚀,其余复垦模式未观察到明显细沟侵蚀;5)产流速率与水流功率、雷诺数(R2>0.998)呈极显著的线性关系,产沙速率与水流功率(R2 >0.733)、雷诺数(R2>0.744)呈极显著的幂函数、指数函数关系。该研究可为铁尾矿坡面的复垦模式选择提供理论依据。

       

      Abstract: Abstract: Reclamation is a key measure to ameliorate soil erosion from slopes in mining tailings. However, how rainfall intensity and different reclamation patterns combine to affect soil erosion remains elusive, especially in the loess plateau in China. We experimentally investigated these using artificial slopes in iron ore tailings as an example. The experiment was conducted in laboratory using a rainfall simulator. We compared three rainfall intensities, 60, 90 and120 mm/h, and five remediation methods: iron ore tailings without adding any amendment (T), overlaying the iron ore tailings with a high proportion of soil (TSH), planting mushroom in the iron ore tailings (TM), overlaying soil on the iron ore tailings and planting mushroom in the soil (TSM); overlaying a low proportion of soil on the iron ore tailings (TST). The experiment for each treatment was conducted in a 2 m × 1 m × 2.3 m soil flume, in which a layer of iron ore tailings 40 cm thick was underlaid by a 20 cm of above remediating substrate. The cultivar of the vegetation was Lespedeza bicolor Turcz. The angle between the soil flume to the horizontal was 25o. The soil water content in all treatments prior to rainfall was the same. During the experiment, we measured the water flow velocity and collected sediment samples after each three minutes to calculate the surface runoff and sediment erosion rate. The hydraulic parameters were also calculated in attempts to determine its impact on sediment erosion. The results showed: 1) The surface runoff rate increased asymptotically with time and it was higher in treatments with mushroom than those without mushroom. 2) The mushroom had a significant impact on sediment erosion. Regardless of rainfall density, the sediment erosion rate decreased with time in treatments with mushroom while increased with time in treatments without mushroom, especially in TSL. Soil erosion in T was most sensitive to rainfall intensity and it increased with rainfall intensity. 3) Water flow was laminar in most cases. Except in TSH under moderate and high rainfall intensity and T under high rainfall intensity where water flow was supercritical, water flow in other treatments was subcritical. The average infiltration depth in all treatments was shallow and ranged from 0.23 to 0.93 mm. The Manning roughness coefficient and the Darcy-Weisbach friction of the remediating substrates planted with mushroom were higher than that without mushroom. Mushroom reduced water velocity but increased the surface roughness compared to those without mushroom. 4) Splash erosion and shear erosion was the main cause of sediment erosion. 5) The runoff rate was linearly related to the stream power and to the Reynolds number with R2>0.998. The erosion rate was related to the steam power exponentially with R2>0.733 and to the Reynolds number in a power-law with R2>0.744. This study improves our understanding of how different mediating methods and rainfall density combine to impact surface runoff and sediment erosion in slopes in iron or tailings.

       

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